Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley

Includes bibliography. === The pilot balloon runs and synoptic charts show that mountain and valley winds at the Jonkershoek valley correspond with the west to east ridging of anticyclones over the South Western Cape. Saddles between the South Atlantic and South Indian anticyclones are particularly...

Full description

Bibliographic Details
Main Author: Ngeleza, Eric B
Other Authors: Washington, R
Format: Dissertation
Language:English
Published: University of Cape Town 2015
Subjects:
Online Access:http://hdl.handle.net/11427/13420
id ndltd-netd.ac.za-oai-union.ndltd.org-uct-oai-localhost-11427-13420
record_format oai_dc
spelling ndltd-netd.ac.za-oai-union.ndltd.org-uct-oai-localhost-11427-134202020-10-06T05:11:22Z Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley Ngeleza, Eric B Washington, R Environmental and Geographical Science Includes bibliography. The pilot balloon runs and synoptic charts show that mountain and valley winds at the Jonkershoek valley correspond with the west to east ridging of anticyclones over the South Western Cape. Saddles between the South Atlantic and South Indian anticyclones are particularly conducive to the development of well established local wind circulations at Jonkershoek. Gradient winds during the occurrence of saddles are shown to be light and variable. Deep gradient southeasterlies undergo an acceleration to the lee of the ridges resulting in strong airflow at the Jonkershoek valley bottom. The topography at Jonkershoek is shown not have any meaningful modifying effect on the gradient northwesterlies. 2015-07-14T08:42:09Z 2015-07-14T08:42:09Z 1993 Master Thesis Masters MSc http://hdl.handle.net/11427/13420 eng application/pdf University of Cape Town Faculty of Science Department of Environmental and Geographical Science
collection NDLTD
language English
format Dissertation
sources NDLTD
topic Environmental and Geographical Science
spellingShingle Environmental and Geographical Science
Ngeleza, Eric B
Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
description Includes bibliography. === The pilot balloon runs and synoptic charts show that mountain and valley winds at the Jonkershoek valley correspond with the west to east ridging of anticyclones over the South Western Cape. Saddles between the South Atlantic and South Indian anticyclones are particularly conducive to the development of well established local wind circulations at Jonkershoek. Gradient winds during the occurrence of saddles are shown to be light and variable. Deep gradient southeasterlies undergo an acceleration to the lee of the ridges resulting in strong airflow at the Jonkershoek valley bottom. The topography at Jonkershoek is shown not have any meaningful modifying effect on the gradient northwesterlies.
author2 Washington, R
author_facet Washington, R
Ngeleza, Eric B
author Ngeleza, Eric B
author_sort Ngeleza, Eric B
title Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
title_short Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
title_full Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
title_fullStr Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
title_full_unstemmed Modification of gradient winds by dissected topography in the vicinity of the Jonkershoek Valley
title_sort modification of gradient winds by dissected topography in the vicinity of the jonkershoek valley
publisher University of Cape Town
publishDate 2015
url http://hdl.handle.net/11427/13420
work_keys_str_mv AT ngelezaericb modificationofgradientwindsbydissectedtopographyinthevicinityofthejonkershoekvalley
_version_ 1719348962785230848